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View article: Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel
Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel Open
Subglacial environments comprise ∼10 % of Earth's land surface, host active microbial ecosystems, and are important components of global biogeochemical cycles. However, the broadly inaccessible nature of subglacial systems has left them va…
View article: Comment on tc-2022-240
Comment on tc-2022-240 Open
Abstract. Subglacial environments comprise ~10 % of Earth’s land surface, host active microbial ecosystems, and are important components of global biogeochemical cycles. However, the broadly inaccessible nature of subglaci…
View article: Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel
Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel Open
Subglacial environments comprise ~10 % of Earth’s land surface, host active microbial ecosystems, and are important components of global biogeochemical cycles. However, the broadly inaccessible nature of subglacial systems has left them va…
View article: Supplementary material to "Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel"
Supplementary material to "Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel" Open
Methods S1: Water isotope fractionation modelA model was developed using the principles of isotopic fractionation to estimate the isotopic composition of incremental ice, incremental vapor, and residual water as a hydraulically isolated wa…
View article: Subglacial Deformation of Permafrost Beneath Wright Lower Glacier, Antarctica as Revealed by Direct Observations and Measurements from a Subglacial Tunnel
Subglacial Deformation of Permafrost Beneath Wright Lower Glacier, Antarctica as Revealed by Direct Observations and Measurements from a Subglacial Tunnel Open
View article: Canadian high arctic ice core records of organophosphate flame retardants and plasticizers
Canadian high arctic ice core records of organophosphate flame retardants and plasticizers Open
Arctic ice cap cores were analyzed for organophosphate esters (OPEs). Depositional flux increased exponentially over 4 decades at one site but were lower further north. Some OPEs were associated with anthropogenic particles, possibly micro…
View article: Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel
Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel Open
Geochemical data for the paper "Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel"
View article: Scott Polar Research Institute Arctic Airborne Radio-Echo Sounding Datasets: Canadian Arctic 2000
Scott Polar Research Institute Arctic Airborne Radio-Echo Sounding Datasets: Canadian Arctic 2000 Open
This data set contains radar sounder profiles from the SPRI 100 MHz ice-penetrating radar instrument over Devon and Ellesmere islands in the Canadian Arctic (CA). Along with the radar profile data, the archive includes derived and ancillar…
View article: Arctic Report Card 2020: Glaciers and Ice Caps Outside of Greenland
Arctic Report Card 2020: Glaciers and Ice Caps Outside of Greenland Open
View article: The Arctic
The Arctic Open
peer reviewed
View article: Ice Core Record of Persistent Short‐Chain Fluorinated Alkyl Acids: Evidence of the Impact From Global Environmental Regulations
Ice Core Record of Persistent Short‐Chain Fluorinated Alkyl Acids: Evidence of the Impact From Global Environmental Regulations Open
Short chain perfluoroalkylcarboxylic acids (scPFCAs, C x F 2x+1 COOH, x ≤ 3) are persistent compounds formed from atmospheric oxidation of fluorotelomer compounds and chlorofluorocarbon (CFC) replacements introduced as a result of the Mont…
View article: Classification of glaciers during summer in Southern Rocky Mountain Trench using surface albedo and temperature anomalies
Classification of glaciers during summer in Southern Rocky Mountain Trench using surface albedo and temperature anomalies Open
<p>Under most atmospheric conditions, the albedo and temperature of surface snow and ice are two of the main influences on the energy budget for glacier melting. Given that surface albedo and temperature are linked, knowing where and…
View article: Basal thermal regime affects the biogeochemistry of subglacial systems
Basal thermal regime affects the biogeochemistry of subglacial systems Open
Ice formed in the subglacial environment can contain some of the highest concentrations of solutes, nutrients, and microbes found in glacier systems, which can be released to downstream freshwater and marine ecosystems and glacier forefiel…
View article: Basal thermal regime affects the biogeochemistry of subglacial systems
Basal thermal regime affects the biogeochemistry of subglacial systems Open
Ice formed in the subglacial environment can contain some of the highest concentrations of solutes, nutrients, and microbes found in glacier systems. Upon glacial melt, these materials are released to downstream freshwater and marine ecosy…
View article: Proglacial freshwaters are significant and previously unrecognized sinks of atmospheric CO <sub>2</sub>
Proglacial freshwaters are significant and previously unrecognized sinks of atmospheric CO <sub>2</sub> Open
Significance Glacier melt is one of the most dramatic consequences of climate change in high-latitude and high-altitude environments. As meltwaters move across poorly consolidated landscapes, they transport vast quantities of highly reacti…
View article: Atmospheric forcing of rapid marine-terminating glacier retreat in the Canadian Arctic Archipelago
Atmospheric forcing of rapid marine-terminating glacier retreat in the Canadian Arctic Archipelago Open
Marine-terminating glaciers in the Canadian Arctic Archipelago have retreated in response to atmospheric, not oceanic, warming.
View article: Influence of recent warming and ice dynamics on glacier surface elevations in the Canadian High Arctic, 1995–2014
Influence of recent warming and ice dynamics on glacier surface elevations in the Canadian High Arctic, 1995–2014 Open
Repeat airborne laser altimetry measurements show widespread thinning (surface lowering) of glaciers in Canada's Queen Elizabeth Islands since 1995. Thinning rates averaged for 50 m elevation bins, were more than three times higher during …
View article: Continuous non-marine inputs of per- and polyfluoroalkyl substances to the High Arctic: a multi-decadal temporal record
Continuous non-marine inputs of per- and polyfluoroalkyl substances to the High Arctic: a multi-decadal temporal record Open
Perfluoroalkyl acids (PFAAs) are persistent, in some cases, bioaccumulative compounds found ubiquitously within the environment. They can be formed from the atmospheric oxidation of volatile precursor compounds and undergo long-range trans…
View article: Discovery of a hypersaline subglacial lake complex beneath Devon Ice Cap, Canadian Arctic
Discovery of a hypersaline subglacial lake complex beneath Devon Ice Cap, Canadian Arctic Open
A possible analog for saline lakes on planetary ice bodies lurks beneath a Canadian Arctic ice cap.
View article: The world’s largest High Arctic lake responds rapidly to climate warming
The world’s largest High Arctic lake responds rapidly to climate warming Open
View article: Spatiotemporal variability of Canadian High Arctic glacier surface albedo from MODIS data, 2001–2016
Spatiotemporal variability of Canadian High Arctic glacier surface albedo from MODIS data, 2001–2016 Open
Inter-annual variations and longer-term trends in the annual mass balance of glaciers in Canada's Queen Elizabeth Islands (QEI) are largely attributable to changes in summer melt. The largest source of melt energy in the QEI in summer is n…
View article: Continuous Non-Marine Inputs of Per- and Polyfluoroalkyl Substances to the High Arctic: A Multi-Decadal Temporal Record
Continuous Non-Marine Inputs of Per- and Polyfluoroalkyl Substances to the High Arctic: A Multi-Decadal Temporal Record Open
Perfluoroalkyl acids (PFAAs) are persistent, bioaccumulative compounds found ubiquitously within the environment. They can be formed from the atmospheric oxidation of volatile precursor compounds and undergo long-range transport through th…
View article: Supplementary material to "Continuous Non-Marine Inputs of Per- and Polyfluoroalkyl Substances to the High Arctic: A Multi-Decadal Temporal Record"
Supplementary material to "Continuous Non-Marine Inputs of Per- and Polyfluoroalkyl Substances to the High Arctic: A Multi-Decadal Temporal Record" Open
View article: 7. Rates of Chemical Weathering in Glaciated Terrain (MT)
7. Rates of Chemical Weathering in Glaciated Terrain (MT) Open
View article: 4. The First Haut Glacier D’arolla Project (MT)
4. The First Haut Glacier D’arolla Project (MT) Open
View article: Glacier Biogeochemistry
Glacier Biogeochemistry Open
This volume charts our interlinked research pathways, which began with an interest in water flow paths at glacier beds and expanded into an exploration of the role of glaciers and ice sheets in local, regional, and global biogeochemical cy…
View article: 10. Life in Subglacial Lakes (MT)
10. Life in Subglacial Lakes (MT) Open
View article: 5. The Second Arolla Project (MS)
5. The Second Arolla Project (MS) Open
View article: 9. Towards the Organic Geochemistry of Glaciers (MS)
9. Towards the Organic Geochemistry of Glaciers (MS) Open
View article: 11. Concluding Remarks (MS and MT)
11. Concluding Remarks (MS and MT) Open